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- W2109541379 abstract "A late Quaternary pollen record from northern Sakhalin Island (51.34°N, 142.14°E, 15 m a.s.l.) spanning the last 43.7 ka was used to reconstruct regional climate dynamics and vegetation distribution by using the modern analogue technique (MAT). The long-term trends of the reconstructed mean annual temperature (TANN) and precipitation (PANN), and total tree cover are generally in line with key palaeoclimate records from the North Atlantic region and the Asian monsoon domain. TANN largely follows the fluctuations in solar summer insolation at 55°N. During Marine Isotope Stage (MIS) 3, TANN and PANN were on average 0.2 °C and 700 mm, respectively, thus very similar to late Holocene/modern conditions. Full glacial climate deterioration (TANN = −3.3 °C, PANN = 550 mm) was relatively weak as suggested by the MAT-inferred average climate parameters and tree cover densities. However, error ranges of the climate reconstructions during this interval are relatively large and the last glacial environments in northern Sakhalin could be much colder and drier than suggested by the weighted average values. An anti-phase relationship between mean temperature of the coldest (MTCO) and warmest (MTWA) month is documented during the last glacial period, i.e. MIS 2 and 3, suggesting more continental climate due to sea levels that were lower than present. Warmest and wettest climate conditions have prevailed since the end of the last glaciation with an optimum (TANN = 1.5 °C, PANN = 800 mm) in the middle Holocene interval (ca 8.7–5.2 cal. ka BP). This lags behind the solar insolation peak during the early Holocene. We propose that this is due to continuous Holocene sea level transgression and regional influence of the Tsushima Warm Current, which reached maximum intensity during the middle Holocene. Several short-term climate oscillations are suggested by our reconstruction results and correspond to Northern Hemisphere Heinrich and Dansgaard–Oeschger events, the Bølling–Allerød and the Younger Dryas. The most prominent fluctuation is registered during Heinrich 4 event, which is marked by noticeably colder and drier conditions and the spread of herbaceous taxa." @default.
- W2109541379 created "2016-06-24" @default.
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- W2109541379 creator A5046346284 @default.
- W2109541379 creator A5052219121 @default.
- W2109541379 creator A5071053676 @default.
- W2109541379 date "2015-05-01" @default.
- W2109541379 modified "2023-09-25" @default.
- W2109541379 title "Late Quaternary vegetation and climate dynamics at the northern limit of the East Asian summer monsoon and its regional and global-scale controls" @default.
- W2109541379 cites W1503731010 @default.
- W2109541379 cites W1542285314 @default.
- W2109541379 cites W1631559605 @default.
- W2109541379 cites W1951064340 @default.
- W2109541379 cites W1968531149 @default.
- W2109541379 cites W1968721411 @default.
- W2109541379 cites W1971635734 @default.
- W2109541379 cites W1974173193 @default.
- W2109541379 cites W1974971410 @default.
- W2109541379 cites W1976328939 @default.
- W2109541379 cites W1977419644 @default.
- W2109541379 cites W1977505730 @default.
- W2109541379 cites W1977972205 @default.
- W2109541379 cites W1978248369 @default.
- W2109541379 cites W1980012339 @default.
- W2109541379 cites W1981309347 @default.
- W2109541379 cites W1984198610 @default.
- W2109541379 cites W1984273454 @default.
- W2109541379 cites W1985949400 @default.
- W2109541379 cites W1987192412 @default.
- W2109541379 cites W1989913318 @default.
- W2109541379 cites W1990899433 @default.
- W2109541379 cites W1992646017 @default.
- W2109541379 cites W1993955673 @default.
- W2109541379 cites W1994007098 @default.
- W2109541379 cites W1995083616 @default.
- W2109541379 cites W1996932107 @default.
- W2109541379 cites W2002054438 @default.
- W2109541379 cites W2002086647 @default.
- W2109541379 cites W2002907989 @default.
- W2109541379 cites W2003501861 @default.
- W2109541379 cites W2004195001 @default.
- W2109541379 cites W2005056929 @default.
- W2109541379 cites W2005192137 @default.
- W2109541379 cites W2005736516 @default.
- W2109541379 cites W2008875043 @default.
- W2109541379 cites W2008953916 @default.
- W2109541379 cites W2011774329 @default.
- W2109541379 cites W2011974751 @default.
- W2109541379 cites W2012914171 @default.
- W2109541379 cites W2014036968 @default.
- W2109541379 cites W2019327536 @default.
- W2109541379 cites W2019558782 @default.
- W2109541379 cites W2023474451 @default.
- W2109541379 cites W2024309015 @default.
- W2109541379 cites W2024369723 @default.
- W2109541379 cites W2027385173 @default.
- W2109541379 cites W2028971837 @default.
- W2109541379 cites W2029122292 @default.
- W2109541379 cites W2035325438 @default.
- W2109541379 cites W2037304784 @default.
- W2109541379 cites W2039630741 @default.
- W2109541379 cites W2039691001 @default.
- W2109541379 cites W2041756570 @default.
- W2109541379 cites W2042399444 @default.
- W2109541379 cites W2048833517 @default.
- W2109541379 cites W2051126029 @default.
- W2109541379 cites W2051467875 @default.
- W2109541379 cites W2054777801 @default.
- W2109541379 cites W2057337344 @default.
- W2109541379 cites W2061303947 @default.
- W2109541379 cites W2064042802 @default.
- W2109541379 cites W2066529619 @default.
- W2109541379 cites W2070396620 @default.
- W2109541379 cites W2076959952 @default.
- W2109541379 cites W2077167883 @default.
- W2109541379 cites W2077600132 @default.
- W2109541379 cites W2078976556 @default.
- W2109541379 cites W2079549096 @default.
- W2109541379 cites W2085809769 @default.
- W2109541379 cites W2086192317 @default.
- W2109541379 cites W2086568086 @default.
- W2109541379 cites W2087928515 @default.
- W2109541379 cites W2088841971 @default.
- W2109541379 cites W2089144464 @default.
- W2109541379 cites W2091324450 @default.
- W2109541379 cites W2099358694 @default.
- W2109541379 cites W2099826005 @default.
- W2109541379 cites W2103737089 @default.
- W2109541379 cites W2103983252 @default.
- W2109541379 cites W2107211406 @default.
- W2109541379 cites W2108888355 @default.
- W2109541379 cites W2110116713 @default.
- W2109541379 cites W2114771431 @default.
- W2109541379 cites W2120637384 @default.
- W2109541379 cites W2128162479 @default.
- W2109541379 cites W2135078263 @default.
- W2109541379 cites W2135758856 @default.